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Impact of climate change on a landslide in South East France, simulated using different GCM scenarios and downscaling methods for local precipitation

机译:气候变化对法国东南部滑坡的影响,使用不同的GCM情景和降尺度方法模拟了当地降水

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ABSTRACT: The aim of this paper is to assess the influence of different climate scenarios on scenarios for the impact variable ?landslide activity1. For this purpose, a site-specific model was used, relating the activity of a landslide in South East France to climate. Landslide activity was reconstructed from tree ring data. Hydrological field data indicated that the controlling climatic variable is net precipitation (precipitation minus evapotranspiration). However, this variable and hence the impact model could not explain all of the variations in landslide activity. The landslide model was fed with 1 temperature and several precipitation scenarios obtained by applying 3 different methods for downscaling 3 different general circulation model (GCM) simulations of the large-scale climate. The skill of the downscaling methods in reproducing the historical local precipitation was either limited or trivial, but fair enough to justify further application. The resulting scenarios for landslide activity were quite similar, with the exception of 2 specific combinations of GCM and downscaling method. Furthermore, short-term climatic variation, plausibly represented in one of the downscaling methods as a random noise component, caused additional variation in the resulting scenarios. The amount of variation in the climate scenarios is of the same order of magnitude as that in the landslide model. The general conclusion is not to focus on calibrating impact models while using only 1 climate scenario, but to assess the overall uncertainty of the impact scenario by considering different parameter settings of the impact model as well as different climate scenarios, as was done in the present study.
机译:摘要:本文的目的是评估不同气候情景对影响变量滑坡活动的情景的影响1。为此,使用了特定地点的模型,该模型将法国东南部的滑坡活动与气候联系起来。滑坡活动是从年轮数据重建的。水文现场数据表明,控制气候变量是净降水量(降水量减去蒸散量)。但是,该变量以及影响模型无法解释滑坡活动的所有变化。滑坡模型具有1个温度,并且通过应用3种不同的方法将大型气候的3种不同的一般环流模型(GCM)模拟降尺度获得了几种降水情景。降尺度方法在再现历史局部降水方面的技能是有限的或微不足道的,但足够合理以证明有必要进一步应用。所产生的滑坡活动情景与GCM和降尺度方法的2种特定组合非常相似。此外,短期气候变化(在一种降尺度方法中合理地表示为随机噪声分量)导致了结果方案中的其他变化。气候情景中的变化量与滑坡模型中的变化量相同。总的结论不是仅在使用一种气候情景时就专注于校准影响模型,而是要像目前所做的那样,通过考虑影响模型的不同参数设置以及不同的气候情景来评估影响情景的总体不确定性。研究。

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